Ensemble estimates reveal a complex hydroclimatic sensitivity of pine growth at Carpathian cliff sites
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F12%3A00186515" target="_blank" >RIV/62156489:43210/12:00186515 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67179843:_____/12:00384015
Výsledek na webu
<a href="http://www.sciencedirect.com/science/article/pii/S0168192312000767" target="_blank" >http://www.sciencedirect.com/science/article/pii/S0168192312000767</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.agrformet.2012.02.011" target="_blank" >10.1016/j.agrformet.2012.02.011</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Ensemble estimates reveal a complex hydroclimatic sensitivity of pine growth at Carpathian cliff sites
Popis výsledku v původním jazyce
Carpathian pine growth at its natural range limit, where small hydroclimatic fluctuations are indicated by tree-ring width anomalies, may provide insight into past ecological responses to climatic changes. Tree-ring chronologies from extreme cliff sitesmay also contain annually resolved and accurately dated information to facilitate the development of palaeoclimatic reconstructions. Complex and spatiotemporally inconsistent relationships between biotic and abiotic factors, however, often complicate ourunderstanding of forest growth dynamics. In this study, we utilized a novel ensemble approach of 3240 growth--climate interactions to evaluate the likelihood of temporal fluctuations in the hydroclimatic sensitivity of three newly developed tree-ring width chronologies from 515 Scots pines (Pinus sylvestris). The data represent undisturbed cliff habitats across the northwestern Carpathian arc between 700 and 1050 m asl. These sites are located in the northern (N) and southern (S) Tatra
Název v anglickém jazyce
Ensemble estimates reveal a complex hydroclimatic sensitivity of pine growth at Carpathian cliff sites
Popis výsledku anglicky
Carpathian pine growth at its natural range limit, where small hydroclimatic fluctuations are indicated by tree-ring width anomalies, may provide insight into past ecological responses to climatic changes. Tree-ring chronologies from extreme cliff sitesmay also contain annually resolved and accurately dated information to facilitate the development of palaeoclimatic reconstructions. Complex and spatiotemporally inconsistent relationships between biotic and abiotic factors, however, often complicate ourunderstanding of forest growth dynamics. In this study, we utilized a novel ensemble approach of 3240 growth--climate interactions to evaluate the likelihood of temporal fluctuations in the hydroclimatic sensitivity of three newly developed tree-ring width chronologies from 515 Scots pines (Pinus sylvestris). The data represent undisturbed cliff habitats across the northwestern Carpathian arc between 700 and 1050 m asl. These sites are located in the northern (N) and southern (S) Tatra
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
GK - Lesnictví
OECD FORD obor
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Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2012
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Agricultural and Forest Meteorology
ISSN
0168-1923
e-ISSN
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Svazek periodika
160
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
10
Strana od-do
100-109
Kód UT WoS článku
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EID výsledku v databázi Scopus
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